Reactive Hydraulic Fracturing Fluid

ABSTRACT

Hydraulic fracturing fluids and methods to hydraulically fracture a subterranean formation and oxidize organic material in the subterranean formation. The hydraulic fracturing fluid includes water, another fluid, and a surfactant. An inorganic oxidizer is included in the water.

TECHNICAL FIELD

This disclosure relates to hydraulic fracturing.

BACKGROUND

Hydraulic fracturing employs fluid and material to generate fractures in a subterranean formation to stimulate production from oil and gas wells. Hydraulic fracturing is a well-stimulation technique in which rock is fractured by a pressurized liquid that may be a fracturing fluid. The process can involve the pressure injection of fracturing fluid into a wellbore to generate cracks in the deep-rock formations through which natural gas, petroleum, and brine will flow more freely. The fracturing typically generates paths that increase the rate at which production fluids, such as crude oil or natural gas, can be produced from the reservoir formations. The amount of increased production may be related to the amount of fracturing. Proppant may be employed to maintain the fractures as pressure depletes in the well during hydrocarbon production. The proppant may resist formation closure stresses to keep fractures open.

Hydraulic fracturing may allow for the recovery of crude oil and natural gas from unconventional formations that geologists once believed were impossible to produce. Unconventional source rocks may be organic-rich sedimentary deposits, such as shales and mud rocks. The organic components of the source shale may include hydrocarbon-source material kerogen and kerogen-produced components bitumen and pyrobitumen.

SUMMARY

An aspect relates to a method of hydraulic fracturing. The method includes providing a hydraulic fracturing fluid through a wellbore into a subterranean formation. The hydraulic fracturing fluid includes water, a nonpolar fluid, and a surfactant. The hydraulic fracturing fluid includes an inorganic oxidizer in the water. The method includes hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid.

Another aspect relates to a method of hydraulic fracturing. The method includes providing a hydraulic fracturing fluid through a wellbore into a subterranean formation. The hydraulic fracturing fluid includes an aqueous phase and a non-aqueous phase. The aqueous phase includes water and an inorganic oxidizer in the water. The method includes hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid. The oxidizing of the organic material degrades the organic material. The organic material includes kerogen.

Yet another aspect relates to a hydraulic fracturing fluid for hydraulic fracturing a subterranean formation. The hydraulic fracturing fluid includes: (1) water at less than 50 volume percent (vol %) of the hydraulic fracturing fluid; (2) a fluid at greater than 50 vol % of the hydraulic fracturing fluid; (3) an inorganic oxidizer in the water at a molality of at least 10 millimolar (mM) in the water; and (4) a surfactant.

The details of one or more implementations are set forth in the accompanying drawings and the description below. Other features and advantages will be apparent from the description and drawings, and from the claims.

BRIEF DESCRIPTION OF DRAWINGS

FIG. 1 is a diagram of a well having a wellbore formed in a subterranean formation having organic matter, such as kerogen.

FIG. 2 a diagram of the well of FIG. 1 after a hydraulic fracture is formed and with the well in production.

FIG. 3 is a diagram of a well employing a hydraulic fracturing fluid that is an oxidizing fracturing fluid having an internal aqueous phase.

FIG. 4 is a diagram of a well employing a hydraulic fracturing fluid that is an oxidizing fracturing fluid having an external aqueous phase.

FIG. 5 is a diagram of a well site having a wellbore formed through the Earth surface into a subterranean formation in the Earth crust.

FIG. 6 is a method of hydraulic fracturing a subterranean formation having organic material.

Like reference numbers and designations in the various drawings indicate like elements.

DETAILED DESCRIPTION

Some aspects of the present disclosure are directed to employing a hydraulic fracturing fluid that is reactive to break down kerogen in a subterranean formation during hydraulic fracturing. Embodiments include hydraulic fracturing fluids that are reactive in bearing an oxidizing component(s) (oxidizer). The hydraulic fracturing fluid also includes water and an additional fluid. The water may have an inorganic oxidizer.

The fluid (in addition to the water) may be gas or hydrophobic liquid (generally immiscible with water), or both. This additional fluid as a gas may be an inert gas (e.g., CO₂) in a nonpolar gas phase of the hydraulic fracturing fluid. The additional fluid as a liquid (generally immiscible with water) may be oil, liquid carbon dioxide (CO₂), or supercritical CO₂, and in a nonpolar phase (non-aqueous phase) of the fracturing fluid. The oil may generally be inert. The oil may be, for example, mineral oil. The supercritical CO₂ may behave as a liquid in certain respects.

An advantage of the present fracturing fluid may include reduction of water use in hydraulic fracturing. Further, if the inert gas or liquid CO₂ (or supercritical CO₂) is employed in the fracturing fluid, another advantage may be the beneficial effect of the inert gas or liquid CO₂ (or supercritical CO₂) on hydrocarbon recovery in displacing hydrocarbons from the kerogen and formation.

The hydraulic fracturing fluid may have an external phase (also labeled as continuous phase or carrier phase) and an internal phase (also labeled as a discontinuous phase or dispersed phase). The fracturing fluid may have a surfactant. The water (aqueous phase) may be the external phase or the internal phase. Again, the water may have an inorganic oxidizer.

The hydraulic fracturing fluid may be a foam, emulsion, foamed emulsion, or liquid-carrying gas. The foam, emulsion, foamed emulsion, or liquid-carrying gas may be reactive or oxidizing.

As indicated, the oxidizer(s) in the fracturing fluid may include an inorganic oxidizer in an aqueous (polar) phase of the fracturing fluid. The fracturing fluid may additionally include an oxidizer in another phase. The other phase may be a non-aqueous phase, hydrophobic phase, nonpolar phase, nonpolar gas phase, nonpolar solvent phase, water-immiscible phase, water-immiscible liquid phase, etc.

In particular for examples with the fracturing fluid having a nonpolar gas phase (e.g., inert gas, such as CO₂), the additional oxidizer may be a reactive gas (e.g., chlorine dioxide) in the nonpolar gas phase. In examples with the fracturing fluid having a water-immiscible phase that is liquid (e.g., hydrophobic liquid such as oil or CO₂) or supercritical (e.g., CO₂), the additional oxidizer may be an organic oxidizer.

The oxidizing fracturing fluid via the oxidizer(s) breaks down kerogen in the subterranean formation during hydraulic fracturing. As mentioned, a benefit may include reduction of water use as compared to typical hydraulic fracturing. Another benefit may be the effect of the non-aqueous phase on hydrocarbon recovery in displacement of hydrocarbons from the kerogen-laden formation.

Production from unconventional source-rock formations has become economically viable. The technology for accessing these reservoirs continues to advance as the industry improves drilling, completion, and stimulation techniques. Unconventional source-rock reservoirs differ from conventional reservoirs at least due to the presence of the hydrocarbon source material (for example, kerogen and kerogen-produced components) in unconventional source-rock reservoirs. This hydrocarbon source material as irregular organic matter can represent, for example, 5-10 weight percent (wt %) of the sedimentary source-rock formation or 10-20 volume percent (vol %) of the sedimentary source-rock formation. An assortment of minerals are woven and compacted together with the organic matter (for example, kerogen) resulting in a complex hierarchical structure with toughness and strength characteristics similar to other natural materials. The tensile characteristics of the organic matter have been demonstrated by nanoindentation of organic-rich shale micro/nano-cantilever source-shale beams tested under a scanning electron microscope (SEM). The chemomechanical characteristics of the organic matter implicate a problematic role of the organic matter in the tensile stresses in hydraulic fracturing and in overall mechanical and chemical operational success of the fracturing. The interwoven organic matter that the fracturing fluid encounters as the fracture extends into the source rock formation is further discussed with respect to FIG. 1.

FIG. 1 is well 100 having a wellbore 102 formed in a subterranean formation 104 having organic matter 106 (organic material), such as kerogen. The wellbore 102 is depicted as a circular cross section. The subterranean formation 104 is a geological formation in the Earth crust and may be an unconventional source-rock formation having hydrocarbon. The subterranean formation 104 may be an organic-rich shale zone. The spider-web symbol represents the presence of the organic matter 106.

In FIG. 1, a fracture 108 is being formed via injection of a fracturing fluid 110 (stimulation fluid) from the Earth surface through the wellbore 102 into the subterranean formation 104. The fracturing fluid 110 may be injected at a specified flow rate (q₀). The flow rate (q₀) may be specified as a volumetric flow rate or mass flow rate. The fracturing fluid 110 may include proppant 112, such as sand or ceramic proppant. The fracture 108 may propagate perpendicular to a minimum principal stress 114 of the formation 104 and in a direction against a maximum principal stress 116 of the formation.

The schematic in FIG. 1 depicts the hydraulic fracture 108 extending from the wellbore 102. The fracturing fluid 110 system encounters the ductile organic matter 106 illustrated as spider webs. The presence of the organic matter 106 at the fracture face 118 may restrict the generation of permeable channels from the subterranean formation 104 into the fracture 108. Thus, the organic matter 106 may inhibit the subsequent production of hydrocarbon from the formation 104 into and through the fracture 108 to the wellbore 102 and Earth surface. The fracture face 118 may be an interface of the forming fracture 108 with the subterranean formation 104. Conventional hydraulic-fracturing stimulation fluids typically do not address challenges of fracturing organic-rich shale zones. The polymer-like organic material 106 may be intertwined within the organic material and with the rock. The organic material 106 affects fracturing (fracture) behavior and reduces resulting hydraulic conductivity.

Hydraulic fracturing fluids may include polymers or crosslinkers for viscosifying the fracturing fluids as proppant-carrying fluids. Fracturing fluids (or stimulation fluid chemicals) may also include additives, such as polymer breakers, biocides, clay swelling inhibitors, and scale inhibitors. Among the most commonly-used fracturing fluids for unconventional formations are slickwater systems incorporating friction-reducing synthetic polymers that facilitate the pumping of stimulation fluids at large rates (for example, at least 100 barrels per minute). Moreover, the incorporation of gas into fracturing fluids may reduce or eliminate water altogether as a component of the fracturing fluid.

To address the challenge of improving hydraulic fracturing in unconventional source-rock reservoirs, embodiments of the present techniques include reactive fluids that can break down the polymer nature of the organic matter 106 on the hydraulic fracture faces 118. At the fracture face 118, organic matter 106 (for example, kerogen) is beneficially cracked or fragmented open due to exposure to oxidizing conditions (for example, aqueous oxidizing conditions). Techniques to implement the oxidizing conditions via a fracturing fluid 110 include a fracturing fluid having, for example, an inorganic oxidizer in aqueous fluid. The fracturing fluid may additionally have an organic oxidizer in oil, liquid CO₂, or supercritical CO2. The fracturing fluid may have a reactive gas (oxidizer) in an inert gas (if employed) of the fracturing fluid.

Thus, the fracturing fluids include reactive fluids having or that are an oxidizer that can break down the polymer nature of the organic matter on the hydraulic fracture faces. The fracturing fluids having an oxidizer(s) can include surfactants to promote forming of a dispersed phase in a continuous phase and keep any proppant suspended. FIG. 2 provides a schematic of kerogen that has cracked open as a result of exposure to oxidizing conditions (for example, aqueous oxidizing conditions). Though the merits of fracturing with an oxidizer-containing fluid generally are indicated, such a fluid if an aqueous fluid relies on freshwater that is sometimes scarce depending on the well location. Further, the use of water in some formations may cause damage. Also, the aqueous fluid itself may have little interaction with the kerogen organic matter. On this point, kerogen holds onto light-chain hydrocarbons. The lack of interaction between water and kerogen may resist displacement of this hydrocarbon by the water. In response, embodiments give a fracturing fluid that can have both water and inert gas, both water and oil, or both water and liquid CO₂. The fracturing fluid may be a foam, an emulsion, a foamed emulsion, or a liquid-carrying gas, and so on.

Embodiments include a hydraulic fracturing fluid (or treatment fluid) having water (aqueous phase) at less than 50 volume percent (vol %), another fluid (e.g., non-aqueous phase) at greater than 50 vol %, and a surfactant. The water may have an inorganic oxidizer. The water (aqueous phase) may be a continuous phase (external phase or carrying phase) in the fracturing fluid or a dispersed phase (internal phase or discontinuous phase) in the fracturing fluid. In some embodiments, the other fluid (e.g., >50 vol %) may be generally immiscible with the water (e.g., <50 vol %) in the fracturing fluid.

The other fluid (e.g., non-aqueous and/or nonpolar) may be a hydrophobic liquid (for example, oil or liquid CO₂) or hydrophobic supercritical fluid (e.g., CO₂), with or without an organic oxidizer. For the other fluid being a liquid (or supercritical fluid) immiscible with water, the fracturing fluid may be an emulsion.

The other fluid may be an inert gas (for example, CO₂, ethane, propane, or nitrogen, or mixtures thereof) with or without a reactive gas as an oxidizer. In examples with the other fluid being inert gas as a dispersed phase, the fracturing fluid may be a foam.

In examples with the other fluid being inert gas as a continuous phase, the inert gas may carry the water, and the fracturing fluid may be labeled as a liquid-carrying gas. The water may be entrained in the inert gas.

For the other fluid including both a gas and a liquid (or supercritical fluid) immiscible with water, the fracturing fluid may be a foamed emulsion. For instance, the gas and the liquid (or supercritical fluid) immiscible with water may be dispersed in the water to form the foamed emulsion.

Additives (for example, a viscosifier) may be incorporated for proppant suspension in fracturing applications at the selected water ratios (for example, water-to-gas ratio). Fluids of this compositional range employ less water than water-based systems, employ less surfactant than typical hydraulic fracturing fluids having surfactant, and accommodate oxidizers of varying solubility arising from the mixed-solvent nature of the fracturing fluid. As indicated, the fracturing fluid may be foam, emulsion, foamed-emulsion, or liquid-carrying gas.

FIG. 2 is a well 200 that is the well 100 of FIG. 1 after the hydraulic fracture 108 is formed and with the well 200 in production. FIG. 2 depicts the hydraulic fracture 108 extending from the wellbore 102. The fracture 108 has a length 202 and width 204. The fracturing fluid 110 (FIG. 1) that formed the fracture 108 was reactive fracturing fluid having an oxidizer that attacked the organic matter 106. Thus, the fracturing fluid 110 caused organic matter 106 to crack open to generate permeable channels from the formation 104 into the fracture 108. Therefore, conductivity is increased from the formation 104 through the fracture 108 into the wellbore 102. The well 200 as depicted is in production phase with produced hydrocarbon 206 flow from the subterranean formation 104 through the fracture 108 and wellbore 102 to the Earth surface. The flow rate of the produced hydrocarbon 206 may be labeled as Qo and may be characterized as a volumetric flow rate or mass flow rate.

As discussed, the present hydraulic fracturing-fluid systems may include a reactive component(s) (one or more oxidizers) for breaking down organic matter 106, such as kerogen, in the subterranean formation 104. Embodiments hydraulically fracture unconventional source-rock formations. These reactive fracturing fluids may contain a specified amount of oxidizer that can break down organic material (for example, kerogen) in the subterranean formation. As for oxidizer selection, the oxidizers employed in this application demonstrate reactivity toward kerogen. To this end, salts of chlorate and bromate are examples. Both are reactive toward kerogen. Further, reactive gases, such as chlorine dioxide, are applicable as oxidizers.

The present hydraulic fracturing fluid includes at least one oxidizer, a surfactant (or amphilic block copolymer), and at least two phases generally immiscible with respect to each other. One phase is a continuous phase (external or carrier phase) and the other phase is a discontinuous phase (internal or dispersed phase). One phase may be hydrophobic and the other phase hydrophilic.

In examples of the fracturing fluid as a foam, the foam may have a nonpolar inert gas (and any reactive gas) as the discontinuous phase in or dispersed in water (aqueous phase) that is the continuous phase. The fracturing fluid as a liquid-carrying gas may have water (aqueous phase) as the discontinuous phase in or dispersed in a nonpolar inert gas (and any reactive gas) that is the continuous phase.

In examples of the fracturing fluid as an emulsion, the emulsion may have a hydrophobic or nonpolar liquid (having an organic oxidizer in some implementations) as the discontinuous phase in or dispersed in water (aqueous phase) that is the continuous phase. The nonpolar liquid may be, for example, oil or CO₂. The CO₂ in the emulsion may be a liquid or supercritical fluid. The supercritical CO2 may resemble a liquid in certain respects, such as in regard to density. In other examples, the fracturing fluid as an emulsion may have the water (aqueous phase) as the discontinuous phase in or dispersed in the nonpolar liquid that is the continuous phase.

In examples of the hydraulic fracturing fluid as a foamed emulsion, the foamed emulsion may include both inert gas and liquid (immiscible with water) dispersed in water. In the foamed emulsion, the water is the continuous phase. The (1) inert gas (optionally having a reactive gas as an oxidizer) and (2) liquid (immiscible with water and optionally having an organic oxidizer) may each be respective discontinuous phases in or dispersed in water (having an organic oxidizer) that is the continuous phase. The liquid immiscible in water may be, for example, oil, liquid CO₂, or supercritical CO₂ (having behaviors of liquid).

In various embodiments of the hydraulic fracturing fluid, a surfactant may absorb to the boundary between two immiscible phases. Surfactant molecules may be amphiphilic in having a hydrophic part (hydrophobic tail) and a hydrophilic part (polar head group). The surfactant may absorb to the interface between a hydrophobic phase (for example, nonpolar gas) and a hydrophilic phase (for example, water). At the interface, the surfactant aligns so that the hydrophobic tail of the surfactant molecule is in the nonpolar gas and the polar head group of the surfactant molecule is in the water. This may cause a decrease in surface or interfacial tensions. The hydrocarbon tail may be, for example, a hydrocarbon, fluorocarbon, or siloxane.

Surfactants may be classified as nonionic, anionic, cationic, or zwitterionic based on the charge of the polar head group. A nonionic surfactant has a polar head group with no charge. Examples of nonionic surfactant include alcohol ethoxylates (AE) including ethoxylated aliphatic alcohols. An anionic surfactant has a polar head group with a negative charge. Examples of anionic surfactant are alkyl sulfates. A cationic surfactant has a polar head group with a positive charge. Examples of cationic surfactant are quaternary ammonium salts. A zwitterionic surfactant has a polar head group with both a positive charge and a negative charge. Examples of zwitterionic surfactant include betaines and amphoacetates.

As indicated, the present techniques may include an oxidizing foam, oxidizing emulsion, oxidizing foamed emulsion, or oxidizing liquid-carrying gas that are utilized as a hydraulic fracturing fluid. The oxidizing foam may be include a gas dispersed in liquid. The oxidizing foam may be a mixture of an inert gas, water, surfactant, and an oxidizer(s). Similarly, the oxidizing liquid-carrying gas may be a mixture of an inert gas, water, surfactant, and an oxidizer(s). The oxidizing liquid-carrying gas may include liquid (water) dispersed in gas (inert gas).

The oxidizing emulsion may include a mixture of two immiscible liquids. The two immiscible liquids may be water and a liquid immiscible with water. The liquid immiscible with water may be, for example, oil or liquid CO₂. The oxidizing emulsion may include a mixture of a liquid (e.g., water) and a supercritical fluid (e.g., CO₂) that are immiscible.

The oxidizing emulsion may be a mixture of water, fluid (liquid or supercritical fluid) that is immiscible with water, a surfactant, and an oxidizer(s). Examples of the present emulsions may include water dispersed in hydrophobic liquid or supercritical fluid (e.g., water-in-supercritical CO₂ microemulsions). Examples of the present emulsions may include hydrophobic liquid dispersed in water.

The hydraulic fracturing fluid as an oxidizing foamed emulsion may include gas (e.g., inert gas) and liquid (generally immiscible with water) both dispersed in water having an inorganic oxidizer. The liquid immiscible with water may be, for example, oil.

The present oxidizing hydraulic-fracturing fluid may break down kerogen in the subterranean formation during the hydraulic fracturing of the subterranean formation while utilizing less water than other hydraulic fracturing fluids. If included in the fracturing fluid, the inert gas, liquid CO₂, or supercritical CO₂ may increase hydrocarbon recovery as compared to hydraulic fracturing fluids without an inert gas, liquid CO₂, or supercritical CO₂. In particular, the inert gas, liquid CO₂, or supercritical CO₂ may promote displacement of hydrocarbons from the subterranean formation including from the kerogen.

FIG. 3 is a well 300 employing a hydraulic fracturing fluid 302 that is a reactive hydraulic-fracturing fluid having at least one oxidizer. The hydraulic fracturing fluid 302 may be formulated and mixed to give the fracturing fluid 302 as reactive at least because of the oxidizer(s). In embodiments, the hydraulic fracturing fluid 302 includes on a volume basis: (1) water less than 30%, less than 25%, or in the range of 5% to 30%, and which may form an internal aqueous phase 304 (dispersed phase) in the oxidizing fracturing fluid; (2) a fluid (e.g., inert fluid) at least 65% or at least 70%, or in the range of 70% to 90%, and which may form an external phase 306 (continuous phase) in the fracturing fluid; and (3) a surfactant or an amphilic block copolymer (or both) less than 5% or in a range of 0.03% to 5%.

The fluid that is the external phase 306 may generally be immiscible with water. The external phase 306 fluid may be gas, liquid, or supercritical fluid.

The external phase 306 fluid may be liquid (e.g., oil or CO₂) or supercritical fluid (e.g., CO₂). If so, the hydraulic fracturing fluid 302 may be an emulsion. The oil may be, for example, mineral oil.

The external phase 306 fluid may be an inert gas. If so, the external phase 306 may be an inert-gas carrier phase, and the hydraulic fracturing fluid 302 labeled as a liquid-carrying gas or water-carrying gas in embodiments. The inert gas may be CO₂, nitrogen (N₂), ethane, propane, butane, or argon, or mixtures of these. The inert gas carries the water. In certain embodiments, the fracturing fluid with the inert gas as the external phase 306 may have characteristics of a mist or aerosol, but in some instances with increased liquid (water) loading in the internal (dispersed) phase 304. In particular embodiments with the external phase 306 as inert gas, the carried or entrained water may be droplets or formed dispersed slugs.

The surfactant 308 may facilitate formation of the fracturing fluid 302 having the external phase 306 (continuous phase) as inert gas, liquid (e.g., oil or CO₂), or supercritical fluid (e.g., CO₂). In the illustrated embodiment, the external phase 306 may generally be immiscible with water. The surfactant 308 may be an interfacial surfactant (as depicted) in the fracturing fluid 302. The surfactant 308 may be a pseudo-surfactant that is an amphilic block copolymer (also known as amphiphilic block copolymer) that functions as an interfacial surfactant in being amphiphilic with hydrophobic block(s) and hydrophilic block(s).

The water includes the inorganic oxidizer at a concentration, for example, in the range of 10 millimolar (mM) to 200 mM in the water or 10 millimolar (mM) to 150 mM in the water. The inorganic oxidizer may be at least 50 mM in the water. The inorganic oxidizer may be in the internal aqueous phase 304 of the formed fracturing fluid 302. The molar concentration of the inorganic oxidizer based on the amount of overall hydraulic fracturing fluid 302 may be less than 75 mM in some implementations. The inorganic oxidizer may be an alkali salt (which may be an alkaline-earth metal salt) having an anion that may be bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.

In the illustrated embodiment, the hydraulic fracturing fluid 302 is reactive (oxidizing) and includes: (a) the internal aqueous phase 304 including water having the inorganic oxidizer; (b) the interfacial surfactant 308; and (c) the external phase 306 (as the continuous phase) optionally having an oxidizer as a second oxidizer in the fracturing fluid 302.

The second oxidizer (if employed) may be included in the fracturing fluid 302 to reside in the external phase 306. For examples of the external phase 306 as an inert gas, the second oxidizer may be a reactive gas. The reactive gas may include, for example, chlorine dioxide, bromine, ozone, or chlorine. In examples of the external phase 306 as oil or CO₂ (liquid CO₂ or supercritical CO₂), the second oxidizer may be an organic oxidizer.

For the external phase 306 as oil, liquid CO₂, or supercritical CO₂, the second oxidizer may be an organic oxidizer, such as in having an organic cation. The organic oxidizer with the organic cation may have an inorganic anion as the oxidizer. The second oxidizer may be quaternary ammonium salts of the following anions: bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite. The second oxidizer may be salts of pyridinium, pyrrolidinium, imidazolium, tetraphenylphosphonium, or bis(triphenylphosphine)iminium paired with one of the following anions: bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite.

If the second oxidizer (organic oxidizer or reactive gas) is included, the molality of total oxidizer (inorganic oxidizer plus second oxidizer) in the fracturing fluid 302 may be, for example, in the range of 10 mM to 150 mM. The unit mM for this molality range of total oxidizer is moles of total oxidizer per kilogram of fracturing fluid 310. The total oxidizer may be the combined amount of the inorganic oxidizer (as a first oxidizer) in the water and the second oxidizer in the external phase 306.

A simplified schematic of a wellbore 310 in a subterranean formation 312 is depicted. In the illustrated implementation, the wellbore 310 has a casing 314. Surface equipment includes pump(s) to introduce the fracturing fluid 310 through the wellbore 310 into the subterranean formation 312. For examples of the external gas phase 306 as inert gas (and thus the hydraulic fracturing fluid 310 having a gas content of at least 70 vol %), the pump(s) may be configured for multi-phase flow including with relatively high gas content.

The surfactant 308 (for example, interfacial surfactant) to promote the fracturing fluid 302 having the external continuous phase 306 and internal (dispersed) aqueous phase 304 may be a cationic surfactant, an anionic surfactant, a nonionic surfactant, or a zwitterionic surfactant. This surfactant (for example, the interfacial surfactant 308) to make the emulsion or liquid-carrying gas may be fluorinated as in the following examples: (1) perfluoroether ammonium carboxylate or ammonium carboxylic acid perfluoroether; (2) (C₇F₁₅CH(OSO₃Na⁺)C₇H₁₅ (a double-tail hybrid fluorocarbon/hydrocarbon surfactant); (3) bis(1H,1H,5H-octafluoro-n-pentyl) sodium sulfosuccinate (di-HCF4); (4) sodium 1-oxo-1-[4-(perfluorohexyl)phenyl]hexane-2-sulfonate, FC6-HC4; (5) 1-oxo-1-[4-(perfluorohexyl)phenyl]hexane (Nohead FC6HC4); (6) sodium 1,5bis[(1H,1H,2H,2H-perfluorobutyl)oxy]-1,5-dioxopentane-2-sulfonate (2FG(EO)₂); (7) sodium 1,5-bis[(1H,1H,2H,2H-perfluorohexyl)oxy]-1,5dioxopentane-2-sulfonate (4FG(EO)₂); (8) sodium 1,5-bis[(1H,1H,2H,2H-perfluorodecyl)oxy]-1,5-dioxopentane-2-sulfonate (8FG(EO)₂); (9) sodium 1,4-bis[(1H,1H,2H,2H-perfluorohexyl)oxy]-1,4dioxobutane-2-sulfonate (4FS(EO)₂); and (10) sodium 1,4-bis[(1H,1H,2H,2H-perfluorodecyl)oxy]-1,4-dioxobutane-2-sulfonate (8FS(EO)₂). The surfactant (for example, the interfacial surfactant 308) to make the water-in-inert gas foam or emulsion may also be nonfluorinated as in the case of poly(ethylene glycol) 2,6,8-trimethyl-4-nonyl ethers, such as octa(ethylene glycol) 2,6,8-trimethyl-4-nonyl ether (5b-C₁₂E₈). The amphilic block-copolymer (functioning as a surfactant 108) can be fluorinated or non-fluorinated as in the case of F(CF₂CF₂)₃₋₈CH₂CH₂O(CH₂CH₂O)₁₀₋₁₅H and poly(ethylene oxide)-b-poly(butylene oxide), respectively.

The hydraulic fracturing fluid 302 may include additives, such as a clay inhibitor, buffer, scale inhibitor, flowback enhancer, corrosion inhibitor, or fluid loss agent, or any combinations of these. The water (for example, the water that forms into the internal aqueous phase 304) added to the hydraulic fracturing fluid 302 may have a viscosifier (for example, a polysaccharide) to increase viscosity of the fracturing fluid 302. One example of polysaccharide as a viscosifier is guar or guar gum (also called guaran), which is a galactomannan polysaccharide. The fracturing fluid 302 may have a friction reducer to decrease friction experienced by the fracturing fluid 302 in the pumping of the fracturing fluid through the wellbore into the subterranean formation. The friction reducer may be, for example, an anionic copolymer.

The viscosifier or friction reducer, or both, may be added with the water or separate from the water to the fracturing fluid 302. Once added and mixed with the fracturing fluid, the viscosifier or friction reducer, or both, may reside generally exclusively or predominantly in the internal aqueous phase 304.

FIG. 4 is a well 400 including a hydraulic fracturing fluid 402 that is reactive or oxidizing fracturing fluid. The hydraulic fracturing fluid 402 may be formulated and mixed to give the hydraulic fracturing fluid 402 as the reactive (oxidizing) fracturing fluid. In embodiments, the hydraulic fracturing fluid 402 as formulated includes on a volume basis: (1) water less than 50% or less than 45% or in range of 10% to 45%, and which may form an external aqueous phase 404; (2) a fluid (e.g., inert fluid) greater than 45%, greater than 50%, or greater than 55%, or in a range of 50% to 80% or range of 50% to 90%, and which may form an internal phase 406 in the oxidizing hydraulic fracturing fluid 402; and (3) a surfactant or an amphilic block copolymer (or both) less than 5% or in a range of 0.03% to 5%. The water includes an inorganic oxidizer. Therefore, the external aqueous phase 404 may be characterized as an external aqueous oxidizer phase.

The water includes the inorganic oxidizer at a concentration, for example, in the range of 10 millimolar (mM) to 150 nM in the water (based on the amount of water) in the external aqueous phase 404 of the fracturing fluid 402. The molar concentration (molality) of the inorganic oxidizer based on the amount of overall hydraulic fracturing fluid 402 may be less than 75 mM in some implementations. The inorganic oxidizer may be an alkali salt (including an alkaline-earth metal salt) of the following anions: bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.

Options for the fluid as the internal phase 406 include: (a) inert gas to form the fracturing fluid 402 as foam; (b) oil, liquid CO₂, or supercritical CO₂ to form the fracturing fluid 402 as an emulsion; or (c) both oil and inert gas to form the fracturing fluid 402 as a foamed emulsion. With respect to the foamed emulsion, the internal phase 406 can be two respective internal phases 406 including an oil phase and an inert-gas phase. For the fracturing fluid 402 as foam or foamed emulsion, the inert gas may be CO₂, N₂, ethane, propane, butane, or argon, or mixtures of these.

The inert gas in the foam can have a reactive gas as an oxidizer. The oil, liquid CO₂, or supercritical CO₂ in the emulsion can have an organic oxidizer as an oxidizer in the fracturing fluid 402. As for the foamed emulsion, the oil phase and the inert-gas phase may each have a respective oxidizer. For this foamed emulsion, the oxidizer (if employed) in the oil phase may be an organic oxidizer, and the oxidizer (if employed) in the inert gas may be a reactive gas.

The surfactant (or amphilic block copolymer) in the fracturing fluid 402 may facilitate formation of fracturing fluid 402 as the foam, emulsion, or foamed emulsion, and with the water as the continuous phase. The surfactant (or amphilic block copolymer) may be the interfacial surfactant 408 as depicted in the oxidizing fracturing fluid 402. The surfactant (for example, as the interfacial surfactant 408) may promote formation of the fracturing fluid 402 giving the aqueous continuous phase may be a cationic compound, an anionic compound, a nonionic compound, or a zwitterionic compound. For instance, the surfactant betaines, sulfated or sulfonated alkoxylates, alkyl quarternary amines, alkoxylated linear alcohols, alkyl sulfonates, alkyl aryl sulfonates, or C10-C20 alkyldiphenyl ether sulfonates. The surfactant 408 may be polyethylene glycols, ethers of alkylated phenol, sodium dodecylsulfate, alpha olefin sulfonates (for example, sodium dodecane sulfonate), and trimethyl hexadecyl ammonium bromide. In implementations, the surfactant (which may arrange as the interfacial surfactant 408) may be added to the fracturing fluid 402 in concentrations in the range from about 0.05% to about 2% by weight of the liquid in the fracturing fluid 402. The concentration of the surfactant may be from about 0.5 gallons to about 20 gallons per 1000 gallons of liquid in the fracturing fluid 402.

In the illustrated embodiment, the hydraulic fracturing fluid 402 (oxidizing) includes: (a) the external aqueous phase 404 (as the continuous phase) having an inorganic oxidizer; (b) the internal phase 406 optionally having an oxidizer (e.g., as a second oxidizer in the fracturing fluid 402); and (c) the interfacial surfactant 408. A simplified schematic of a wellbore 410 in a subterranean formation 412 is depicted. In the illustrated implementation, the wellbore 410 has a casing 414.

As indicated, the internal phase 406 may optionally have an oxidizer (e.g., as a second oxidizer of the hydraulic fracturing fluid 402). This second oxidizer (if included) may be incorporated in the fracturing fluid 402 to reside in the internal phase 406.

For examples of hydraulic fracturing fluid 402 as an oxidizing foam with the internal phase 406 including inert gas, the additional oxidizer may be a reactive gas. The reactive gas may be, for example, chlorine dioxide, bromine, ozone, or chlorine. This reactive gas as an oxidizer that may be optionally included in the inert gas in the fracturing fluid 402 may be a second oxidizer of the fracturing fluid 402.

For examples of hydraulic fracturing fluid 402 as an oxidizing emulsion with the internal phase 406 including oil, liquid CO₂, or supercritical CO₂, the oxidizer in the internal phase 406 as a second oxidizer of the fracturing fluid 402 may be an organic oxidizer. This organic oxidizer may have an organic cation and oxidizing inorganic anion. If so, the oxidizing inorganic anion may be, for example, a bromate ion or a chlorate ion. The organic oxidizer in the internal phase 406 of the emulsion may be quaternary ammonium salts of the following anions: bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite. The organic oxidizer may be salts of pyridinium, pyrrolidinium, imidazolium, imidazolium, tetraphenylphosphonium, or bis(triphenylphosphine)iminium paired with one of the following anions: bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite.

For examples of hydraulic fracturing fluid 402 as an oxidizing foamed emulsion, one or two oxidizers may be included in the two internal phases 404, respectively. The two oxidizers may be a second oxidizer and third oxidizer, respectively, of the fracturing fluid 402. The two oxidizers may be a reactive gas in the inert-gas phase and an organic oxidizer in the oil phase, respectively. As for these oxidizers in addition to the inorganic oxidizer in the water, the foamed emulsion may include one or both of these additional oxidizers in the internal phase 406. For instance, the foamed emulsion may include a reactive gas in the inert gas or an inorganic oxidizer in the oil, or both.

If the second oxidizer is included in the foam, emulsion, or foamed emulsion, or if the second oxidizer and third oxidizer are included in the foamed emulsion, the molality of total oxidizer may be, for example, in the range of 10 mM to 150 mM in which the unit mM here is moles of oxidizer per kilogram of fracturing fluid 402. The total oxidizer may be the combined amount of the inorganic oxidizer (as a first oxidizer of the fracturing fluid) in the water and the second oxidizer (of the fracturing fluid) in the foam, emulsion, or foamed emulsion. In some embodiments of the foamed emulsion, the total oxidizer may be the combined amount of the inorganic oxidizer (as a first oxidizer) in the water, the second oxidizer, and the third oxidizer.

The hydraulic fracturing fluid 402 may include additives, such as a clay inhibitor, buffer, scale inhibitor, flowback enhancer, corrosion inhibitor, or fluid loss agent, or any combinations of these. The water (for example, the water that forms into the external aqueous phase 404) added to the hydraulic fracturing fluid 402 may have a viscosifier (for example, a polysaccharide) or friction reducer. The viscosifier (or friction reducer) may be added with or separate from the water to the fracturing fluid 402. The viscosifier (or friction reducer) may reside in the external aqueous phase 404. One example of polysaccharide as a viscosifier is guar or galactomannan polysaccharide.

Referring to FIGS. 3 and 4, nanoparticles with hydrophobic or hydrophilic properties or with both hydrophobic and hydrophilic domains may be added to the oxidizing fracturing fluid 302, 402 to further stabilize the fracturing fluid 302, 402. Moreover, the type of surfactant 308, 408 utilized (added to the fracturing fluid) may be alternated during pumping of the fracturing fluid to alternate formation of the type of external-phase fracturing fluid. For instance, the type of surfactant may be alternated in examples of the fracturing fluid 302, 402 having an inert gas to alternate the external phase between water 404 and gas 306.

In certain embodiments, the hydraulic fracturing fluid (foam, emulsion, foamed emulsion, or liquid-carrying gas) may be prepared by mixing the inorganic oxidizer and surfactant together in water and optionally with other additives. The other additives may include, for example, viscosifier, crosslinker, clay inhibitor, buffer, scale inhibitor, flowback enhancer, corrosion inhibitors, and fluid loss agents. The addition of the nonpolar fluid (inert gas, oil, liquid CO₂, or supercritical CO₂) may be added subsequently in another mixing step in some embodiments.

There may be advantages of employing this oxidizing fracturing fluid (with an aqueous inorganic oxidizer and optionally an oxidizer in a nonpolar phase) instead of the water alone as the base fluid or the nonpolar fluid alone as the base fluid. The presence of both water and nonpolar fluid facilitates a variety of oxidizers or blends of oxidizers to be utilized. Some oxidizers are only soluble in water while others are only soluble in organic or nonpolar solvents. Embodiments facilitate various oxidizers (including combinations of oxidizers) to be incorporated in the fracturing fluid. In some instances, blends of oxidizer may be beneficial.

The present hydraulic fracturing fluid may synergistically improve or increase the effectiveness of the oxidizer toward the kerogen. The nonpolar fluid has the potential to displace methane and other light hydrocarbons from the kerogen and rock matrix to increase or improve production. Kerogen may absorb CO₂ and other nonpolar fluid but will generally exclude water due to kerogen hydrophobicity. Water alone generally cannot sufficiently flush hydrocarbon (for example, natural gas having economic value) out of the kerogen. The inclusion of both nonpolar solvent (for example, inert gas, oil, liquid CO₂, supercritical CO₂) and polar solvent (for example, water) in the fracturing fluid may improve or increase penetration of the fracturing fluid into the kerogen (or other organic material) in the subterranean formation in the hydraulic fracturing. Having both types of solvents (water and nonpolar solvent) present may help solubilize the various kerogen breakdown products.

Hydraulic fracturing can be water intensive. Some subterranean formations are adversely sensitive to water due, for example, to clay components in the subterranean formation. Further, treatment of flowback water adds cost. In response, the present oxidizing-fracturing fluid treatment may employ less water than traditional hydraulic fracturing treatment. Reduction of the amount of water utilized for hydraulically fracturing may be beneficial.

In embodiments, the viscosity of the oxidizing fracturing fluid may be less viscous than some conventional fracturing fluids. Therefore, for some implementations, treatment pressures of the hydraulic fracturing can be less due to reduced breakdown pressure. This can reduce cost because the fracturing treatment may be less energy-intensive with less breakdown pressure. Increased fracturing efficiency generally results from decreased breakdown pressure for the subterranean formation being subjected to the fracturing.

Viscosity, surface tension, and other colligative properties of the fracturing fluid may affect the rate at which the fracturing fluid permeates the pores of a formation, which in turn can affect the fracturing efficiency. The reducing of fracturing-fluid viscosity with the present fracturing fluid as compared to traditional fracturing fluids may speed the rate of permeation of the fracturing fluid.

The oxidizing fracturing fluid may be less viscous due to the presence of the nonpolar solvent (e.g., nonpolar gas) in the fracturing fluid (e.g., oxidizing foam or emulsions). The structure (for example, multi-scale, foam structure, or emulsion structure) may contribute to proppant suspension, which can lead to less viscosifier employed to facilitate suspension of proppant in the fracturing fluid. The aqueous fluid (containing the inorganic oxidizer) of the fracturing fluid can be viscosified and then foamed or emulsified to provide fracturing fluid with greater viscosity capable of carrying proppants. In certain embodiments for the present fracturing fluid, crosslinked fluids can be foamed or emulsified containing the oxidizers discussed.

FIG. 5 is a well site 500 having a wellbore 502 formed through the Earth surface 504 into a subterranean formation 506 in the Earth crust. The subterranean formation 906 may be labeled as a geological formation, a rock formation, or a hydrocarbon formation. The subterranean formation 506 may be an unconventional formation to be subjected to hydraulic fracturing.

The wellbore 502 can be vertical, horizontal, or deviated. The wellbore 502 can be openhole but is generally a cased wellbore. The annulus between the casing and the formation 506 may be cemented. Perforations may be formed through the casing and cement into the formation 506. The perforations may allow both for flow of hydraulic fracturing fluid into the subterranean formation 506 and for flow of produced hydrocarbon from the subterranean formation 506 into the wellbore 502.

The well site 500 may have a hydraulic fracturing system including a source 508 of hydraulic fracturing fluid 510 at the Earth surface 504 near or adjacent the wellbore 502. The source 508 may include one or more vessels holding the fracturing fluid 510. The fracturing fluid 510 may be stored in vessels or containers on ground, on a vehicle (for example, truck or trailer), or skid-mounted. The fracturing fluid 510 may be a water-based fracturing fluid. In some implementations, the fracturing fluid 510 is slickwater that may be primarily water (for example, at least 98.5% water by volume). The fracturing fluid 510 can be prepared from seawater. The fracturing fluid 510 can also be gel-based fluids. The fracturing fluid 510 can include polymers and surfactants. The fracturing fluid 510 can be a viscoelastic surfactant (VES)-based fluid including a reactive VES-based fracturing fluid having an inorganic oxidizer salt. Additives to the fracturing fluid 510 may include hydrochloric acid, friction reducer, emulsion breaker, emulsifier, temperature stabilizer, and crosslinker. Fracturing fluids 510 of differing viscosity may be employed in the hydraulic fracturing. The fracturing fluid 510 may include proppant. In the illustrated embodiment, the fracturing fluid 510 is an oxidizing fracturing fluid (for example, fracturing fluid 302 or 404) for at least a portion of the hydraulic fracturing. This oxidizing fracturing fluid 510 may be foam, emulsion, foamed emulsion, or liquid-carrying gas.

The hydraulic fracturing system at the well site 500 may include motive devices such as one or more pumps 512 to pump (inject) the fracturing fluid 510 through the wellbore 502 into the subterranean formation 506. The pumps 512 may be, for example, positive displacement pumps and arranged in series or parallel. The wellbore 502 may be a cemented cased wellbore and have perforations for the fracturing fluid 510 to flow (injected) into the formation 506. In some implementations, the speed of the pumps 510 may be controlled to give desired flow rate of the fracturing fluid 510. The system may include a control component to modulate or maintain the flow of fracturing fluid 510 into the wellbore 502 for the hydraulic fracturing. The control component may be, for example, a control valve(s). In some implementations, as indicated, the control component may be the pump(s) 512 as a metering pump in which speed of the pump 512 is controlled to give the desired or specified flow rate of the fracturing fluid 510. The set point of the control component may be manually set or driven by a control system, such as the control system 514.

The hydraulic fracturing fluid 510 may be prepared (formulated and mixed) offsite prior to disposition of the fracturing fluid 510 into the source 508 vessel at the well site 500. Alternatively, a portion (some components) of the fracturing fluid 510 may be mixed offsite and disposed into the source 508 vessel and the remaining portion (remaining components) of the fracturing fluid 510 added to the source 508 vessel or to a conduit conveying the fracturing fluid 510. In other implementations, the fracturing fluid 510 may be prepared onsite with components added to (and batch mixed in) the source 508 vessel.

For embodiments of the fracturing fluid 510 as an oxidizing fracturing fluid, the fracturing fluid 510 in the source 508 vessel may have all components of the fracturing fluid 510. In certain embodiments, some components of the fracturing fluid 510 may be added to the source 508 vessel near or at the time (or during) the pumping of the fracturing fluid 510 into the wellbore 502 for the hydraulic fracturing. In some embodiments, not all components of the fracturing fluid 510 are included in the source 508 vessel. Instead, at least one component of the fracturing fluid 510 is added to a conduit conveying the fracturing fluid 510 either on the suction side of the pump(s) 512 or on the discharge side of the pump(s) 512, or both, as the fracturing fluid 510 is being pumped into the wellbore 502.

An additive or component 516 may be added to the fracturing fluid 508. For the oxidizing fracturing fluid, the component 516 may be, for example, the first oxidizer, the second oxidizer, the third oxidizer, surfactant, or a viscosifier. The concentration of the component 516 in the fracturing fluid 510 may be maintained or adjusted by modulating a flow rate (mass or volume) of addition of the component 516 via a control device 518. The set point of the control device 518 may be manually set or specified (directed) by the control system 514. The control device 518 may be a control valve on the conduit conveying the component 516 to the source 508 (for example, vessel) of the fracturing fluid 510. In some implementations, the component 516 may in an aqueous solution added to the fracturing fluid 510 in the source 508 vessel. Further, instead of adding the component 516 to the source 508 vessel, the component 516 may be added to the discharge conduit of the pump 512 as the pump 512 is providing the fracturing fluid 510 into the wellbore 502.

The hydraulic fracturing system at the well site 500 may have a source of proppant, which can include railcars, hoppers, containers, or bins having the proppant. Proppant may be segregated by type or mesh size (particle size). The proppant can be, for example, sand or ceramic proppants. The source of proppant may be at the Earth surface 504 near or adjacent the wellbore 502. The proppant may be added to the fracturing fluid 510 such that the fracturing fluid 510 includes the proppant. In some implementations, the proppant may be added (for example, via gravity) to a conduit conveying the frac fluid 510, such as at a suction of a fracturing fluid pump 512. A feeder or blender may receive proppant from the proppant source and discharge the proppant into pump 512 suction conduit conveying the fracturing fluid 510.

The fracturing fluid 510 may be a foamed and/or emulsified slurry having the solid proppant. The slurry may be a water-carrying inert gas having proppant. The pump 512 discharge flow rates (frac rates) may include a slurry rate which may be a flow rate of the fracturing fluid 510 having proppant as a foamed slurry, emulsion slurry, foamed emulsion slurry or water-carrying inert gas slurry. The pump 512 discharge flow rates (frac rates) may include a clean rate which is a flow rate of fracturing fluid 510 without proppant. In particular implementations, the fracturing system parameters adjusted may include at least pump(s) 512 rate, proppant concentration in the frac fluid 510, component 516 addition rate, and component 516 concentration in the fracturing fluid 510. Fracturing operations can be manual or guided with controllers.

The well site 500 may include a control system 514 that supports or is a component of the hydraulic fracturing system. The control system 514 includes a processor 520 and memory 522 storing code 524 (logic, instructions) executed by the processor 520 to perform calculations and direct operations at the well site 500. The processor 520 may be one or more processors and each processor may have one or more cores. The hardware processor(s) 520 may include a microprocessor, a central processing unit (CPU), a graphic processing unit (GPU), a controller card, or other circuitry. The memory may include volatile memory (for example, cache and random access memory (RAM)), nonvolatile memory (for example, hard drive, solid-state drive, and read-only memory (ROM)), and firmware. The control system 514 may include a desktop computer, laptop computer, computer server, programmable logic controller (PLC), distributed computing system (DSC), controllers, actuators, or control cards. In operation, the control system 514 may facilitate processes at the well site 500 and including to direct operation of aspects of the hydraulic fracturing system.

The control system 514 may be communicatively coupled to a remote computing system that performs calculations and provides direction. The control system 514 may receive user input or remote-computer input that specifies the set points of the control device 518 or other control components in the hydraulic fracturing system. The control system 514 may specify the set point of the control device 518 for the component 516 addition. In some implementations, the control system 514 may calculate or otherwise determine the set point of the control device 518. The determination may be based at least in part on the operating conditions of the hydraulic fracturing and in certain instances on information (or feedback) regarding the amount of kerogen in the region of the subterranean formation 506 being hydraulically fractured.

The fracturing fluid containing oxidative materials may be applied (pumped) without other hydraulic fracturing fluids employed in the hydraulic fracturing. In other words, the oxidizing fracturing fluid may be pumped as a stand-alone hydraulic fracturing treatment to fracture the formation and in some cases to transport proppant. However, the oxidizing fracturing fluid may also be applied (pumped) in tandem (in a sequence) with other fluids including other hydraulic fracturing fluids.

For instance, the oxidizing fracturing fluid and proppant may be pumped alternately with the oxidizing fracturing fluid without proppant as a hybrid treatment. The oxidizing fracturing fluid may also be pumped as part of a high conductivity channel frac (a channel fracturing operation). Channel fracturing may refer to hydraulic fracturing treatment employing intermittent pumping of proppant-laden fluid and proppant-free fluid to generate conductive channels within the subterranean formation.

In another instance, the present oxidizing fracturing fluid may be pumped in sequence with a VES-based fracturing fluid as the alternate fracturing fluid. The VES fracturing fluid is provided through the wellbore into the subterranean formation to hydraulically fracture the subterranean formation to form hydraulic fractures in the subterranean formation. In implementations, the VES fracturing fluid may be a reactive VES fracturing fluid. The VES fracturing fluid for hydraulic fracturing the subterranean formation may include an inorganic oxidizer salt in addition to the viscoelastic surfactant. If implemented, the method includes oxidizing organic material in the hydraulic fractures with the reactive VES fracturing fluid.

The present oxidizing fracturing fluid (e.g., oxidizing foam, oxidizing emulsion, oxidizing foamed emulsion, or a liquid-carrying gas that is oxidizing) may be pumped alternatively with CO₂-based fluids. A benefit of employing a CO₂-based fracturing fluid in tandem with the present oxidizing fracturing fluid is that CO₂ slugs can promote expulsion of hydrocarbons from the formation. Further, CO₂-based fracturing fluid may include an oxidizer to break down organic material (kerogen) in the formation. CO₂ slugs may enhance delivery of oxidizer to the kerogen. The oxidizer in the CO₂-based fluid may be an oxidizer that is soluble in organic solutions or nonpolar media (solvents) because the CO₂-based fracturing fluid may generally be nonpolar. These oxidizers in the alternate CO₂-based fluid may include an organic cation and an oxidizer inorganic anion. The oxidizer inorganic anion may be, for example, chlorate or bromate. Other oxidizer inorganic anions of the oxidizer in the CO₂-based fracturing fluid may include persulfate, perborate, percarbonate, hypochlorite, peroxide, or iodate.

Another implementation of a CO₂-based fracturing fluid that may be sequenced with the present oxidizing fracturing fluid is supercritical CO₂ fracturing fluid. This alternate supercritical CO₂ fracturing-fluid may have reactive oxidizer gases (for example, bromine, chlorine, chlorine dioxide, or ozone) for the treatment of kerogen-containing rocks to enhance hydraulic fracturing efficiency of unconventional source rock formations. The reactive oxidizer gases (whether included in the sequenced supercritical CO₂ or in the inert gas of the present oxidizing fracturing fluid, or both) may chemically degrade kerogen to enhance rock fracability and clean fracture faces to increase permeability and decrease proppant embedment. The reactive gases may be suited for sequenced CO₂-based fracturing fluids (and for the inert-gas phase in embodiments of the present fracturing fluid) because unlike conventional oxidizers, the reactive oxidizer gases here are generally soluble in nonpolar solvents. The oxidizing gas as molecules may exist as a gas or supercritical fluid (at conditions in the subterranean formation) that is soluble in supercritical CO₂ and has a standard redox potential in excess of 1 volt. Subterranean formation conditions may be, for example, temperature greater than 200° F. and pressure greater than 3000 pounds per square inch gauge (psig). These reactive gases if employed in the sequenced supercritical CO₂ or in the present oxidizing fracturing fluid include, for example, bromine (Br₂), chlorine (Cl₂), fluorine (F₂), chlorine monofluoride (ClF), chlorine dioxide (ClO₂), oxygen (O₂), ozone (O₃), nitrous oxide (N₂O), or nitrite (NO₂) gases.

Reactive gases may also be generated in situ upon injection of precursors with CO₂ into the formation. In such an implementation for a sequenced CO₂-based fracturing fluid, the technique may involve mixing of supercritical CO₂ with an oxidizing gas stream. These oxidizing gas chemicals can be mixed on-the-fly with liquid CO₂ and surfactant to form the sequenced supercritical CO₂ emulsion and pumped. The oxidant (oxidizer) should be consumed downhole and therefore may beneficially preclude flowback treatment or disposal. If the oxidant is prepared in situ for the sequenced supercritical CO₂, the precursors may be injected with supercritical CO₂. For example: (1) the first precursor with CO₂ is injected, (2) a CO₂ spacer is then pumped, and (3) the second precursor with CO₂ is then injected. This order may prevent or reduce premature reaction of the precursors to form the reactive gas.

For bromine as the reactive gas (for the sequenced CO₂ or the present fracturing fluid, or both), the bromine reacts with the kerogen and pyrite. The bromine may partially depolymerize the kerogen (a geopolymer). This reaction of bromine with kerogen may form light-chain products that escape when the CO₂ or inert gas is vented. This reaction of bromine with kerogen may also form a brominated kerogen tar at least partially soluble in CO₂. This kerogen tar may be soluble in hydrocarbons and therefore leave the rock matrix migrating from the formation to the wellbore.

As for supply of ClO₂ as an oxidizer in the supercritical CO₂ or in the inert gas of embodiments of the above-discussed oxidizing fracturing fluid, ClO₂ generators commercially available may be deployed at the well site. The ClO₂ gas can be mixed with the liquid CO₂ or oxidizing on-the-fly for the stimulation and treatment of organic-rich shale formation for enhanced hydrocarbon production. The ClO₂ gas generally does not hydrolyze when entering water and remains a dissolved gas in solution. The ClO₂ gas may be up to 10 times more soluble in water than is chlorine and therefore a greater dose (compared to chlorine) of the oxidizer gas ClO₂ can be delivered to the formation. In lieu of relying on ClO₂ generators, the ClO₂ gas may instead be generated in situ (downhole in the wellbore) via, for example, utilizing sodium chlorite. Over time, produced ClO₂ gas may help degrade the kerogen and increase production. If ClO₂ is the oxidant (oxidizer), ClO₂ may be prepared on site and utilized as a mixture with air.

Lastly, other CO₂-based hydraulic fracturing fluids may be employed in tandem with the present oxidizing fracturing fluid. For example, CO₂-based fluids with an oxidizer containing in-situ forming halogens may be employed. Implementations of generating halogen in situ may include, for example: (1) delivery of encapsulated salts of polyhalogen anions, which decompose at reservoir temperatures to yield the free halogen; (2) generation of bromine, chlorine, and/or iodine by reaction of encapsulated [XO₃]⁻ (X=Cl, Br, I) with encapsulated acids to yield unstable HXO₃, which rapidly decomposes to X₂; (3) generation of bromine, chlorine, and/or iodine by reduction of encapsulated [XO₃]⁻ (X=Cl, Br, I) to form X₂; and (4) use of N-bromosuccinimide, N-chlorosuccinimide, or N-iodosuccinimide as halogenating agents, giving the effect of the free halogen while avoiding environmental concerns.

FIG. 6 is a method 600 of hydraulically fracturing a subterranean formation. The subterranean formation includes organic material, such as kerogen. A wellbore (formed in the subterranean formation) provides access to the subterranean formation.

At block 602, the method includes preparing a hydraulic fracturing fluid having water and a fluid (e.g., non-aqueous phase or nonpolar phase) generally immiscible with water. The water may be an aqueous phase or polar phase. The fluid may be a non-aqueous phase or a nonpolar phase. The fluid may be a hydrophobic liquid or nonpolar solvent (for example, oil, liquid CO₂, supercritical CO₂, etc.) or an inert gas (for example, nonpolar inert gas). The inert gas may be, for example, CO₂, N₂, ethane, propane, butane, or argon, or mixtures thereof. In implementations, the fluid (e.g., non-aqueous phase) is at least 50 vol % of the hydraulic fracturing fluid and the water is less than 50 vol % of the hydraulic fracturing fluid. In other implementations, the fluid (e.g., non-aqueous phase) is at least 70 vol % of the hydraulic fracturing fluid and the water is less than 30 vol % of the hydraulic fracturing fluid.

The hydraulic fracturing fluid may be prepared as a foam, emulsion, foamed emulsion, or liquid-carrying gas. A surfactant may be incorporated into the formulation to promote (as an interfacial surfactant) the forming of the hydraulic fracturing fluid as a foam, emulsion, foamed emulsion, or liquid-carrying gas. The surfactant may be, for example, less than 5 vol % of the hydraulic fracturing fluid.

An inorganic oxidizer is incorporated into the hydraulic fracturing fluid. Thus, the hydraulic fracturing fluid is an oxidizing fracturing fluid. The concentration of the inorganic oxidizer in the water in the hydraulic fracturing fluid may be, for example, in the range of 10 mM to 200 mM or in the range of 10 mM to 150 mM. In certain implementations, the inorganic oxidizer has an anion that is bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.

The surfactant and mixing of the hydraulic fracturing fluid may give generation of the oxidizing fracturing fluid having at least two phases. One phase can be an aqueous phase having the water and the inorganic oxidizer. The other phase can be a nonpolar phase or non-aqueous phase (e.g., inert gas, nonpolar fluid, nonpolar solvent, oil, liquid CO₂, supercritical CO₂, etc.). The oxidizing fracturing fluid may be prepared with the aqueous phase as a continuous external phase and the non-aqueous phase as not a continuous phase but instead an internal phase of the hydraulic fracturing fluid. On the other hand, the oxidizing fracturing fluid may be prepared with the non-aqueous phase as a continuous external phase (a carrier phase) and the aqueous phase as not a continuous phase but instead an internal phase of the hydraulic fracturing fluid.

Whether the continuous phase is aqueous or non-aqueous may depend on the particular surfactant (or type of surfactant) utilized. Other factors contributing to whether the continuous phase is aqueous or non-aqueous may include, for example, the relative amounts of water and non-aqueous fluid in the hydraulic fracturing fluid.

In some implementations, the preparing of the hydraulic fracturing fluid includes mixing the water, the surfactant, and the inorganic oxidizer to give a first mixture. The mixing may be performed in a vessel. One or more additives (for example, viscosifier) may also be included in the forming (mixing) that gives the first mixture. Then, a non-aqueous fluid (e.g., inert gas or non-polar solvent) is added (injected) and mixed with the first mixture to give the hydraulic fracturing fluid. This subsequent addition may be performed in the same vessel or a different vessel. The injection of the non-aqueous fluid (for example, at a given velocity) may promote mixing of the non-aqueous fluid with the first mixture. Mixing may also be implemented by a mechanical rotating agitator, such as an impeller, turbine, propeller, or paddle. While vessel(s) may be utilized, a component(s) may be added online (on-the-fly), such as to a conduit conveying the fracturing fluid.

In certain implementations, a reactive gas as an optional oxidizer is added to the inert gas (if employed) as the non-aqueous fluid prior to addition or injection of the inert gas or is added directly to the hydraulic fracturing fluid. Thus, the non-aqueous phase (for example, nonpolar gas phase) in embodiments of the oxidizing fracturing fluid may include the inert gas and also a reactive gas as an oxidizer. In a particular implementation with chlorine dioxide (ClO₂) as the reactive gas, a ClO₂ generator deployed at the well site supplies the ClO₂ for addition in forming the hydraulic fracturing fluid.

In other implementations with the non-aqueous fluid as oil, liquid CO₂, or supercritical CO₂, then an oxidizer compound (for example, a salt) having an organic cation and an inorganic oxidizer anion may be optionally incorporated to reside in the non-aqueous phase formed in the oxidizing fracturing fluid.

The preparation of the oxidizing hydraulic fracturing fluid may include adding proppant to the hydraulic fracturing fluid (e.g., foam, emulsion, foamed emulsion, or liquid-carrying gas). The oxidizing fracturing fluid may include the proppant for at least a portion of time the oxidizing fracturing fluid is utilized in the hydraulic fracturing of the subterranean formation.

At block 604, the method includes providing (for example, pumping) the hydraulic fracturing fluid through the wellbore into the subterranean formation to hydraulically fracture the subterranean formation. The hydraulic fracturing generates hydraulic fractures in the subterranean formation. The pump(s) (if employed) may be, for example, a positive displacement pump.

The method optionally includes alternating or sequencing the oxidizing hydraulic fracturing fluid with another hydraulic fracturing fluid. For instance, the method may include providing (pumping) a slickwater fracturing fluid through the wellbore into the subterranean formation before (and after) providing the oxidizing fracturing fluid through the wellbore into the subterranean formation. The slickwater fracturing fluid may also include an oxidizer. The method may include pumping a slickwater fracturing fluid through the wellbore into the subterranean formation in sequence with the pumping of the present oxidizing fracturing fluid, where the oxidizing fracturing fluid has proppant.

The method may include alternating providing a CO₂-based fracturing fluid through the wellbore into the subterranean formation with the providing of the present oxidizing fracturing fluid through the wellbore into the subterranean formation. The CO₂-based fracturing fluid may also have an oxidizer to oxidize the organic material in the region of the subterranean formation being subjected to hydraulic fracturing and including in the hydraulic fractures.

At block 606, the method includes oxidizing the organic material (for example, including kerogen) in the subterranean formation with the hydraulic fracturing fluid, such as in the forming hydraulic fractures. The oxidizing may be, for example, via the inorganic oxidizer in the water of the fracturing fluid. The oxidizing of the organic material may degrade or fragment the organic material. Organic material at fracture faces of the hydraulic fractures may be fragmented via the oxidation to create permeable channels through the organic material from the subterranean formation into the hydraulic fractures. Therefore, conductivity of hydrocarbon flow (during subsequent production) from the subterranean into the hydraulic fractures and through the wellbore to the Earth surface may be increased.

At block 608, the method may further include in addition to hydraulic fracturing, the production of hydrocarbon from the subterranean formation. The method may include producing hydrocarbon from the subterranean formation through the permeable channels (for example, block 606) and hydraulic fractures generated to the wellbore.

Lastly, additional discussion in provided with respect to block 602 in the preparing of the hydraulic fracturing fluid. A variation may involve adding or injecting the non-aqueous fluid into the water to give a first mixture and mixing the surfactant and the inorganic oxidizer with the first mixture to give the hydraulic fracturing fluid. Another variation is mixing the surfactant with the water to give a first mixture, injecting the non-aqueous fluid into the first mixture to give a second mixture, and mixing the inorganic oxidizer with the second mixture to give the hydraulic fracturing fluid. Yet another variation is mixing the inorganic oxidizer with the water to give a first mixture, adding or injecting the non-aqueous fluid into the first mixture to give a second mixture, and mixing the surfactant with the second mixture to give the hydraulic fracturing fluid.

The preparing of the hydraulic fracturing fluid may include specifying a concentration of the optional oxidizer (for example, salt or reactive gas) in the non-aqueous phase or in the oxidizing fracturing fluid based at least in part on an amount of kerogen in the subterranean formation. Likewise, the preparing of the hydraulic fracturing fluid may include specifying a concentration of the first oxidizer (inorganic oxidizer) in the water or in the oxidizing fracturing fluid based at least in part on an amount of kerogen in the subterranean formation. The concentration of the oxidizers in the oxidizing fracturing fluid can depend on the quantity of kerogen or other organic matter in the reservoir rock in the subterranean formation, such as in the region of the subterranean formation being subjected to hydraulic fracturing with the oxidizing fracturing fluid. The concentration of the inorganic oxidizer in the water in the oxidizing fracturing fluid to implement can be determined (specified) based on the particular inorganic oxidizer selected and on the amount and type of kerogen in the subterranean formation. Similarly, the concentration of oxidizer (if present) in the non-aqueous phase in the oxidizing fracturing fluid to implement can be determined (specified) based on the particular oxidizer selected and on the amount and type of kerogen in the subterranean formation. Source-rock samples collected from the subterranean formation being hydraulically fractured or to be hydraulically fractured can be collected and analyzed. Laboratory tests (for instance, including etching) can be performed on kerogen embedded in rock surfaces of the samples. Further, the weight percent of the total organic carbon (TOC) in the formation can be determined, for example, via a TOC analyzer or pyrolysis unit. The amount of kerogen in the subterranean region of the subterranean formation to be hydraulically fractured can be calculated, determined, or estimated.

The amount of pyrite or other iron sulfides in the subterranean formation may also be considered in specifying the concentration of the inorganic oxidizer in the water in the oxidizing fracturing fluid and in specifying the concentration of the oxidizer (if employed) in the non-aqueous phase of the oxidizing fracturing fluid. The weight percent of iron sulfide in the formation can be determined, for example, by testing the source-rock samples employing x-ray fluorescence, x-ray diffraction, or energy dispersive x-ray spectroscopy. The amount of kerogen or iron sulfide can also be taken, deduced, or inferred from well logs in certain instances. The determining or specifying the inorganic oxidizer concentration can account for the amount of inorganic oxidizer (or other oxidizer) beneficial to degrade the organic material including kerogen while also accounting for the iron sulfide present in the formation.

The rock surface area within the fracture network that the oxidizing will make contact in the formation can be considered with respect to specifying concentration of the inorganic oxidizer (or other oxidizer) in the oxidizing fracturing fluid. The expected size of the fracture network and the resulting surface area of the fractured zones can be estimated. Other factors relevant in determining or calculating the amount (concentration) of inorganic oxidizer or other oxidizer to specify in the oxidizing fracturing fluid may include any organic components in the fluid downhole and the amount of fluid downhole (including in the wellbore) at the time of placing the oxidizing fracturing fluid through the wellbore into the subterranean formation.

As for surfactant, the addition of the surfactant may generally involve incorporating the surfactant as a component of the hydraulic fracturing fluid before providing or pumping the hydraulic fracturing fluid through the wellbore to the subterranean formation. However, the surfactant may be added to the hydraulic fracturing fluid during the pumping of the hydraulic fracturing fluid. For example, surfactant may be added to a vessel at the well site upstream of the pump. In another instance, the surfactant may be added to a conduit on the suction side of the pump(s) or to a conduit on a discharge side of the pump(s). A reason for such on-the-fly addition may be to alternate the particular surfactant or surfactant type added to the fracturing fluid. The preparing or application of the hydraulic fracturing fluid may involve alternating between adding a first surfactant to the hydraulic fracturing fluid and adding a second surfactant to the hydraulic fracturing fluid. The first surfactant gives the non-aqueous phase as a continuous phase of the oxidizing fracturing fluid and with the aqueous phase as not a continuous phase of the oxidizing fracturing fluid. The second surfactant gives the aqueous phase as a continuous phase of the oxidizing fracturing fluid and with the non-aqueous phase as not a continuous phase of the oxidizing fracturing fluid.

An embodiment is a method of hydraulic fracturing. The method includes providing a hydraulic fracturing fluid through a wellbore into a subterranean formation. The hydraulic fracturing fluid includes water, a nonpolar fluid, and a surfactant. The hydraulic fracturing fluid includes an inorganic oxidizer in the water. The concentration of the inorganic oxidizer in the water may be in a range of 10 mM to 200 mM, and wherein the inorganic oxidizer may have an anion that is bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate. The method includes hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid. In some examples, the nonpolar fluid may be an inert gas. If so, the hydraulic fracturing fluid may include foam or a liquid-carrying gas. A reactive gas that is an oxidizer may be included in the inert gas. The foam generally has the water as an external phase and the inert gas as an internal phase. The hydraulic fracturing fluid may be a liquid-carrying gas with the inert gas as a continuous phase and the water as a dispersed phase. In certain examples, the nonpolar fluid may be oil, liquid carbon dioxide, or supercritical carbon dioxide. If so, the hydraulic fracturing fluid may include an emulsion of the water with the oil, the liquid carbon dioxide, or the supercritical carbon dioxide. An organic oxidizer may be included in the nonpolar fluid. In implementations, the organic oxidizer (if utilized) may have an organic cation and an inorganic anion. The concentration of the surfactant in the hydraulic fracturing fluid ma be less than 5 volume percent (vol %) in certain implementations. The surfactant may be an interfacial surfactant that promotes the hydraulic fracturing fluid having at least two phases, and wherein the two phases are an aqueous phase and a nonpolar phase, respectively. In implementations, the hydraulic fracturing fluid has an aqueous phase and a nonpolar phase. The nonpolar phase may an external phase in the hydraulic fracturing fluid, and the aqueous phase may be an internal phase in the fracturing fluid. On the other hand, the aqueous phase may be an external phase in the hydraulic fracturing fluid, and the nonpolar phase is an internal phase in the fracturing fluid. In some implementations, the nonpolar fluid is at least 50 vol % of the hydraulic fracturing fluid, wherein the water is less than 50 vol % of the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid has an aqueous phase and a non-aqueous phase, wherein the aqueous phase includes the water and is a continuous phase of the hydraulic fracturing fluid, and wherein the non-aqueous phase includes the nonpolar fluid and is not a continuous phase of the hydraulic fracturing fluid. In certain implementations, the nonpolar fluid is at least 70 vol % of the hydraulic fracturing fluid, wherein the water is less than 30 vol % of the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid has an aqueous phase and a non-aqueous phase, wherein the non-aqueous phase includes the nonpolar fluid and is a continuous phase of the hydraulic fracturing fluid, and wherein the aqueous phase includes the water and is not a continuous phase of the hydraulic fracturing fluid. In particular implementations, the may include preparing the hydraulic fracturing fluid, wherein the preparing involves mixing the water, the surfactant, and the inorganic oxidizer to give a first mixture, and injecting the nonpolar fluid into the first mixture, wherein the nonpolar fluid includes an inert gas. In these particular implementations, the method may involve adding a reactive gas that is an oxidizer to the inert gas, and wherein mixing the water, the surfactant, and the inorganic oxidizer includes mixing the water, the surfactant, the inorganic oxidizer, and an additive to give the first mixture.

Another embodiment is a method of hydraulic fracturing. The method includes providing a hydraulic fracturing fluid through a wellbore into a subterranean formation. The hydraulic fracturing fluid includes an aqueous phase and a non-aqueous phase. The aqueous phase includes water and an inorganic oxidizer in the water. In implementations, the non-aqueous phase may be at least 45 vol % of the hydraulic fracturing fluid. The method includes hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid. The oxidizing of the organic material degrades the organic material. The organic material includes kerogen. The method may include specifying a concentration of the inorganic oxidizer in the water or in the hydraulic fracturing fluid based at least in part on an amount of kerogen in the subterranean formation, wherein a molality of the inorganic oxidizer in the water is in a range of 10 millimolar (mM) to 200 nM, and wherein the inorganic oxidizer includes an anion that is bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.

The non-aqueous phase may be an external phase of the hydraulic fracturing fluid, and the aqueous phase an internal phase of the hydraulic fracturing fluid. On the other hand, the non-aqueous phase may be an internal phase of the hydraulic fracturing fluid, and the aqueous phase an external phase of the hydraulic fracturing fluid, and wherein the fracturing fluid includes a foam, an emulsion, or a foamed emulsion. In implementations, the non-aqueous phase may include an inert gas, such as inert gas comprises carbon dioxide (CO₂), nitrogen (N₂), ethane, propane, butane, or argon, or mixtures thereof. If so, the hydraulic fracturing fluid may include a foam, wherein the non-aqueous phase is an internal phase of the hydraulic fracturing fluid, and wherein the concentration of the water in the hydraulic fracturing fluid is less than 50 vol %. In implementations, the non-aqueous phase is an external phase of the hydraulic fracturing fluid, wherein the aqueous phase is an internal phase of the hydraulic fracturing fluid, and wherein the concentration of the water in the hydraulic fracturing fluid is less than 30 vol %. In particular implementations, the non-aqueous phase may have a reactive gas that is an oxidizer. In one implementation, the method includes: adding chlorine dioxide (ClO₂) to the hydraulic fracturing fluid from a ClO₂ generator deployed at a well site of the wellbore; and incorporating at least a majority of the ClO₂ into the non-aqueous phase as a reactive gas that is an oxidizer. The hydraulic fracturing fluid may include an emulsion, and wherein the non-aqueous phase includes oil, liquid CO₂, or supercritical CO₂. If so, the non-aqueous phase may have an organic oxidizer having an organic cation and an oxidizing inorganic anion. In examples, the hydraulic fracturing fluid may include a foamed emulsion, wherein the aqueous phase is an external phase of the hydraulic fracturing fluid, wherein the non-aqueous phase includes a first non-aqueous phase and a second non-aqueous phase that are internal phases of the hydraulic fracturing fluid, the first non-aqueous phase including an inert gas and the second non-aqueous phase including a nonpolar fluid (e.g., oil). The first non-aqueous phase may have a reactive gas as an oxidizer. The second non-aqueous phase may have an organic oxidizer.

The method may include adding proppant to the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid has the proppant for at least a portion of time of providing the hydraulic fracturing fluid through the wellbore into the subterranean formation. The method may include providing a slickwater fracturing fluid through the wellbore into the subterranean formation before providing the hydraulic fracturing through the wellbore into the subterranean formation. In implementations, the slickwater fracturing fluid may have an oxidizer, and wherein the present hydraulic fracturing fluid includes proppant. The method may include providing a CO₂-based fracturing fluid through the wellbore into the subterranean formation before or after the providing the hydraulic fracturing fluid through the wellbore into the subterranean formation. If so, the CO₂-based fracturing fluid in some implementations may have an oxidizer that oxidizes the organic material.

Yet other embodiments include a hydraulic fracturing fluid for hydraulic fracturing a subterranean formation. The hydraulic fracturing fluid includes: (1) water at less than 50 vol % of the hydraulic fracturing fluid; (2) a fluid (e.g., inert and/or immiscible with water) at greater than 45 vol % (at least 45 vol %) of the hydraulic fracturing fluid; (3) an inorganic oxidizer in the water at a molality of at least 10 mM in the water; and (4) a surfactant. The inorganic oxidizer in the water may be an alkali salt having an anion comprising bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate. The concentration of the fluid in the hydraulic fracturing fluid may be at least 65 vol %, and wherein concentration of the water in the hydraulic fracturing fluid may be less than 30 vol %. The hydraulic fracturing fluid may include an internal phase having the fluid and an external aqueous phase having the water and the inorganic oxidizer, and wherein the external aqueous phase is a continuous phase of the hydraulic fracturing fluid. On the other hand, the hydraulic fracturing fluid may have an external phase having the fluid and an internal aqueous phase having the water and the inorganic oxidizer, and wherein the external phase is a continuous phase of the hydraulic fracturing fluid. The fluid may be a nonpolar fluid and is in a non-aqueous phase of the hydraulic fracturing fluid. The fluid may be an inert gas, such as carbon dioxide (CO₂), nitrogen (N₂), ethane, propane, butane, or argon, or mixtures thereof. If so, the fluid may further include a reactive gas as an oxidizer, such as chlorine dioxide, bromine, ozone, or chlorine. In other implementations, the fluid may include oil, liquid CO₂, or supercritical CO₂. If so, the fluid may further include an organic oxidizer. The organic oxidizer may include an organic cation and an inorganic anion. The inorganic anion may include bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite. The organic oxidizer may include a quaternary ammonium salt comprising an anion comprising bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite. The organic oxidizer include a salt having an cation paired with an anion, wherein the cation comprises pyridinium, pyrrolidinium, bis(triphenylphosphine)iminium, imidazolium, or tetraphenylphosphonium, and wherein the anion comprising bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, or nitrite.

The hydraulic fracturing fluid may be a foam, an emulsion, a foamed emulsion, or a liquid-carrying gas. The surfactant may promote formation of the hydraulic fracturing fluid as a foam, an emulsion, a foamed emulsion, or a liquid-carrying gas, and wherein the surfactant may be less than 5 vol % of the hydraulic fracturing fluid. The concentration of the surfactant may be in a range of 0.03 weight percent (wt %) to 2.5 wt % of liquid in the hydraulic fracturing fluid. In some implementations, the surfactant is fluorinated. In other implementations, the surfactant may be an amphilic block copolymer that functions as a surfactant in the hydraulic fracturing fluid. The hydraulic fracturing fluid may have a viscosifier including a polysaccharide that increases viscosity of the hydraulic fracturing fluid, and wherein concentration of the surfactant is in a range of 0.3 gallon to 25 gallons per 1000 gallons of liquid in the hydraulic fracturing fluid.

Yet another embodiment is a method of hydraulic fracturing including providing a hydraulic fracturing fluid through a wellbore into a subterranean formation to hydraulically fracture the subterranean formation. The hydraulic fracturing fluid includes water, an inert gas or liquid, and a surfactant. The hydraulic fracturing fluid includes at least one oxidizer. The at least one oxidizer includes an inorganic oxidizer in the water. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid.

Yet another embodiment is a method of hydraulic fracturing including providing a hydraulic fracturing fluid that is reactive (e.g., oxidizing) through a wellbore into a subterranean formation to hydraulically fracture the subterranean formation. The hydraulic fracturing fluid may be a reactive foam (e.g., oxidizing foam). The hydraulic fracturing fluid may be a reactive emulsion (e.g., oxidizing emulsion). The hydraulic fracturing fluid may be a reactive foamed emulsion (e.g., oxidizing foamed emulsion). The reactive foam (if formed) has a gas phase (having inert gas) and an aqueous phase (having water and an inorganic oxidizer). The gas phase may optionally include a reactive gas as an oxidizer. The method includes oxidizing organic material (including kerogen) in the subterranean formation with the hydraulic fracturing fluid. The oxidizing of the organic material degrades the organic material.

Yet another embodiment relates to method of hydraulic fracturing including pumping a hydraulic fracturing fluid through a wellbore into a subterranean formation to hydraulically fracture the subterranean formation to form hydraulic fractures in the subterranean formation. The hydraulic fracturing fluid includes water, an inert fluid, and an inorganic oxidizer in the water. The method includes adding a surfactant to the hydraulic fracturing fluid to give the hydraulic fracturing fluid as an oxidizing foam, oxidizing emulsion, or oxidizing foamed emulsion. The oxidizing foam (if formed) includes an aqueous phase (having the water and the inorganic oxidizer) and a gas phase (having the inert fluid that is an inert gas). The hydraulic fracturing fluid may optionally include a second oxidizer, such as in the gas phase. For the implementation of the hydraulic fracturing fluid as an oxidizing foam, the inert gas is at least 45 vol % or at least 50 vol % of the hydraulic fracturing fluid. The method includes oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid.

Yet another embodiment is a hydraulic fracturing fluid for hydraulic fracturing a subterranean formation. The hydraulic fracturing fluid is reactive (e.g., oxidizing). The reactive hydraulic fracturing fluid includes water at less than 50 vol % of the hydraulic fracturing fluid, an inert fluid that is at least 50 vol % of the hydraulic fracturing fluid, an inorganic oxidizer in the water at a molality of at least 10 mM in the water, and a surfactant that promotes formation of the hydraulic fracturing fluid as a foam, emulsion, foamed emulsion, or liquid-carrying gas. In implementations, the hydraulic fracturing fluid may optionally include an oxidizer in the inert fluid.

A number of implementations have been described. Nevertheless, it will be understood that various modifications may be made without departing from the spirit and scope of the disclosure. 

1. A method of hydraulic fracturing, comprising: providing a hydraulic fracturing fluid through a wellbore into a subterranean formation, the hydraulic fracturing fluid comprising water, a nonpolar fluid, and a surfactant, wherein the hydraulic fracturing fluid comprises an inorganic oxidizer in the water; hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid; and oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid.
 2. The method of claim 1, wherein the nonpolar fluid comprises an inert gas.
 3. The method of claim 2, wherein the hydraulic fracturing fluid comprises foam with the water as an external phase and the inert gas as an internal phase.
 4. The method of claim 2, wherein the hydraulic fracturing fluid comprises a liquid-carrying gas with the inert gas as a continuous phase and the water as a dispersed phase.
 5. The method of claim 2, wherein the hydraulic fracturing fluid comprises a reactive gas that is an oxidizer in the inert gas.
 6. The method of claim 1, wherein the nonpolar fluid comprises an oil, liquid carbon dioxide, or supercritical carbon dioxide.
 7. The method of claim 6, wherein the hydraulic fracturing fluid comprises an emulsion of the water with the oil, the liquid carbon dioxide, or the supercritical carbon dioxide.
 8. The method of claim 6, wherein the hydraulic fracturing fluid comprises an organic oxidizer in the nonpolar fluid, the organic oxidizer comprising an organic cation and an inorganic anion.
 9. The method of claim 1, wherein concentration of the surfactant in the hydraulic fracturing fluid is less than 5 volume percent (vol %), wherein the surfactant comprises an interfacial surfactant that promotes the hydraulic fracturing fluid comprising two phases, and wherein the two phases comprise an aqueous phase and a nonpolar phase.
 10. The method of claim 1, wherein the nonpolar fluid is at least 50 vol % of the hydraulic fracturing fluid, and wherein the water is less than 50 vol % of the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid comprises an aqueous phase and a non-aqueous phase, wherein the aqueous phase comprises the water and is a continuous phase of the hydraulic fracturing fluid, and wherein the non-aqueous phase comprises the nonpolar fluid and is not a continuous phase of the hydraulic fracturing fluid.
 11. The method of claim 1, wherein the nonpolar fluid is at least 70 vol % of the hydraulic fracturing fluid, wherein the water is less than 30 vol % of the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid comprises an aqueous phase and a non-aqueous phase, wherein the non-aqueous phase comprises the nonpolar fluid and is a continuous phase of the hydraulic fracturing fluid, and wherein the aqueous phase comprises the water and is not a continuous phase of the hydraulic fracturing fluid.
 12. The method of claim 1, wherein the hydraulic fracturing fluid comprises an aqueous phase and a nonpolar phase, wherein the nonpolar phase is an external phase in the hydraulic fracturing fluid, and wherein the aqueous phase is an internal phase in the fracturing fluid.
 13. The method of claim 1, wherein the hydraulic fracturing fluid comprises an aqueous phase and a nonpolar phase, wherein the aqueous phase is an external phase in the hydraulic fracturing fluid, and wherein the nonpolar phase is an internal phase in the fracturing fluid.
 14. The method of claim 1, wherein concentration of the inorganic oxidizer in the water is in a range of 10 millimolar (mM) to 200 mM, and wherein the inorganic oxidizer comprises an anion that is bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.
 15. The method of claim 1, comprising preparing the hydraulic fracturing fluid, wherein preparing comprises mixing the water, the surfactant, and the inorganic oxidizer to give a first mixture, and injecting the nonpolar fluid into the first mixture, wherein the nonpolar fluid comprises an inert gas.
 16. The method of claim 15, comprising adding a reactive gas that is an oxidizer to the inert gas, wherein mixing the water, the surfactant, and the inorganic oxidizer comprises mixing the water, the surfactant, the inorganic oxidizer, and an additive to give the first mixture.
 17. A method of hydraulic fracturing, comprising: providing a hydraulic fracturing fluid through a wellbore into a subterranean formation, the hydraulic fracturing fluid comprising an aqueous phase and a non-aqueous phase, the aqueous phase comprising water and an inorganic oxidizer in the water; hydraulically fracturing the subterranean formation with the hydraulic fracturing fluid; and oxidizing organic material in the subterranean formation with the hydraulic fracturing fluid, wherein oxidizing the organic material comprises degrading the organic material, and wherein the organic material comprises kerogen.
 18. The method of claim 17, comprising specifying a concentration of the inorganic oxidizer in the water or in the hydraulic fracturing fluid based at least in part on an amount of kerogen in the subterranean formation, wherein a molality of the inorganic oxidizer in the water is in a range of 10 millimolar (mM) to 200 nM, and wherein the inorganic oxidizer comprises an anion comprising bromate, chlorate, perchlorate, chlorite hypochlorite, persulfate, iodate, bromite, perborate, dichromate, permanganate, ferrate, percarbonate, nitrite, or nitrate.
 19. The method of claim 17, wherein the non-aqueous phase is an external phase of the hydraulic fracturing fluid, and wherein the aqueous phase in an internal phase of the hydraulic fracturing fluid.
 20. The method of claim 17, wherein the non-aqueous phase is an internal phase of the hydraulic fracturing fluid, wherein the aqueous phase in an external phase of the hydraulic fracturing fluid, and wherein the fracturing fluid comprises a foam, an emulsion, or a foamed emulsion.
 21. The method of claim 17, wherein the non-aqueous phase comprises an inert gas.
 22. The method of claim 21, wherein the inert gas comprises carbon dioxide (CO₂), nitrogen (N₂), ethane, propane, butane, or argon, or mixtures thereof.
 23. The method of claim 21, wherein the hydraulic fracturing fluid comprises foam, wherein the non-aqueous phase is an internal phase of the hydraulic fracturing fluid, and wherein the concentration of the water in the hydraulic fracturing fluid is less than 50 volume percent (vol %).
 24. The method of claim 21, wherein the non-aqueous phase is an external phase of the hydraulic fracturing fluid, wherein the aqueous phase is an internal phase of the hydraulic fracturing fluid, and wherein the concentration of the water in the hydraulic fracturing fluid is less than 30 vol %.
 25. The method of claim 21, wherein the non-aqueous phase comprises a reactive gas comprising an oxidizer.
 26. The method of claim 17, wherein the hydraulic fracturing fluid comprises an emulsion, and wherein the non-aqueous phase comprises oil, liquid CO₂, or supercritical CO₂.
 27. The method of claim 26, wherein the non-aqueous phase comprises an organic oxidizer comprising an organic cation and an oxidizing inorganic anion.
 28. The method of claim 17, wherein the hydraulic fracturing fluid comprises a foamed emulsion, wherein the aqueous phase is an external phase of the hydraulic fracturing fluid, wherein the non-aqueous phase comprises a first non-aqueous phase and a second non-aqueous phase that are internal phases of the hydraulic fracturing fluid, the first non-aqueous phase comprising an inert gas and the second non-aqueous phase comprising a nonpolar fluid.
 29. The method of claim 28, wherein the nonpolar fluid comprises oil.
 30. The method of claim 28, wherein the first non-aqueous phase comprises a reactive gas as an oxidizer.
 31. The method of claim 28, wherein the second non-aqueous phase comprises an organic oxidizer.
 32. The method of claim 17, comprising adding proppant to the hydraulic fracturing fluid, wherein the hydraulic fracturing fluid comprises the proppant for at least a portion of time of providing the hydraulic fracturing fluid through the wellbore into the subterranean formation.
 33. The method of claim 17, comprising providing a slickwater fracturing fluid through the wellbore into the subterranean formation before providing the hydraulic fracturing fluid through the wellbore into the subterranean formation.
 34. The method of claim 33, wherein the slickwater fracturing fluid comprises an oxidizer, and wherein the hydraulic fracturing fluid comprises proppant.
 35. The method of claim 17, comprising providing a CO₂-based fracturing fluid through the wellbore into the subterranean formation before or after the providing the hydraulic fracturing fluid through the wellbore into the subterranean formation.
 36. The method of claim 35, wherein the CO₂-based fracturing fluid comprises an oxidizer that oxidizes the organic material.
 37. The method of claim 17, wherein the non-aqueous phase comprises at least 45 volume percent (vol %) of the hydraulic fracturing fluid.
 38. The method of claim 17, comprising: adding chlorine dioxide (ClO₂) to the hydraulic fracturing fluid from a ClO₂ generator deployed at a well site of the wellbore; and incorporating at least a majority of the ClO₂ into the non-aqueous phase as a reactive gas that is an oxidizer. 39-58. (canceled) 